issues in the comparison of ground gravity with grace data david crossley, saint louis u., dept....
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Issues in the Comparison of Ground Gravity with GRACE DataDavid Crossley, Saint Louis U., Dept. Earth & Atmospheric Science, 3507 Laclede Ave., St. Louis MO 63104 , [email protected].
Jacques Hinderer, EOST, 5 rue Descartes, Strasbourg 67084, France, [email protected],fr
Jurgen Neumeyer, Dept. Geodesy and Remote Sensing, GFZ Potsdam, Germany, [email protected]
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MO Moxa
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Figure 2. Individual station gravity residuals after correcting for local tides, nominal atmospheric pressure loading, and IERS polar motion. Amplitudes are in Gal, with time in days since 1 Jan 2002. Vertical grid marks are semi-annual.
Offsets are critical to long period SG observations and are removed with care. The two series from dual sphere instruments (MO, WE) are treated separately and combined only after all corrections. The linear trend contains secular gravity changes seen by AG instruments and the SG instrument drift.
ACKNOWLEDGEMENTSACKNOWLEDGEMENTS
The ground gravity data is from the ICET database, with other data supplied by: Bernd Richter, Herbert Wilmes, Peter
Wolf, Michel van Camp, and Corinna Kroner. Bernard Ducarme assisted in tidal processing. Jean-Paul Boy provided the hydrology loading. For access to the JPL GRACE data and processing, we thank Frank Lemoine
(NASA), and C. K. Shum and S. C. Han (Ohio State). This research is supported by NSF EAR #0409381 and CNRS.
AGU Session ED03 …AGU Session ED03 …
"The availability of sophisticated large-format printers has created a terrible temptation for scientists to present papers with linear storylines inherited from printed publications. Attending the average poster session becomes the daunting equivalent of reading 10 or
20 papers in less than an hour.“
Principal eigenvector for GRACE data
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GGP stations 1997-2001. Stations BE and PO have stopped, and we did not use ME in this study
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Principal eigenvector for SG data
GRACE gravity field, truncation n = 20
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may 03
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aug 03
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- 11.8 Gal to + 8.2 Gal
Comparison of the first principal eigenvectors and time components that account for 80% variance reduction of the GRACE data and 60% of the SG variability
ABSTRACT AND PROCEDUREABSTRACT AND PROCEDURE
We processed 2 years of SG data from 6 stations in central Europe (Fig. 1) and did an EOF (Empirical Orthogonal Function) analysis to determine the principal
components (PCs) and eigenvectors.
We took GRACE Level 2 monthly satellite solutions, and extracted a portion of the gravity field over the same area as the SG stations. We also did an EOF
analysis of this data.
We compared both gravity field to the predictions of loading from a comprehensive hydrological model.
We computed 3-D atmospheric attraction and deformation as an improvement to our previous empirical admittance -0.3 Gal / hPa (results for only 3 stations
were completed, we do not show them)
OBJECTIVE – TO EXAMINE 3 ISSUESOBJECTIVE – TO EXAMINE 3 ISSUES
Is it possible to compare ground and satellite gravity fields at the precision (Gal) and resolution (10-1000 km) of hydrology? This we have done here.
What is the effect of improving the atmospheric attraction to due a 3-D realistic atmospheric model? This we have done partly.
How should one correct for SG stations that have mass above the gravimeters – thus contributing an additional upwards seasonal effect from soil moisture and snow not seen by the satellite. This we have yet to do.
Station Sensor Offsets removed (Gal) Trend (Gal yr-1)
MB Single sphere 6, from –3.1 to 1.9 Gal 3.86
MC Single sphere 1, at 45.0 Gal 2.31
MO_L Dual sphere, lower 2, from –8.7 to 5.7 Gal 4.83
MO_U Dual sphere, upper 2, from –8.5 to 4.8 Gal 1.95
ST Single sphere none 2.94
VI Single sphere 3, from –1.5 to 4.0 Gal 1.45
WE_L Dual sphere, lower 6, from –41.1 to 5.1 Gal -4.09
WE_U Dual sphere, upper 6, from –43.0 to 7.5 Gal -2.28
LOCAL HYDROLOGYLOCAL HYDROLOGY
The SG data are not corrected for hydrology, which is part of the target signal for GRACE comparisons. Local hydrology
affects SG stations, but if the mass is below the station the local effects should be smoothed by spatial averaging (lots of
instruments).
Comparison between hydrology (soil moisture and snow) loading
in gravity and SG gravity residuals.
GRACE
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Evolution of first GRACE PC with increasing number of months of data showing stability and downward trend in gravity
trend
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Snapshots of SG gravity field, minimum curvature surface
- 5.7 Gal to + 6.9 Gal